
The net uptake of atmospheric carbon dioxide by terrestrial ecosystems, which weakened in 2023.The land carbon sink is the net absorption of carbon dioxide (CO₂) from the atmosphere by terrestrial ecosystems — forests, grasslands, soils, and other vegetation. Through photosynthesis, plants take in CO₂ and convert it into biomass, while respiration and decomposition release some back. The 'sink' refers to the balance: when uptake exceeds release, land acts as a net reservoir for carbon, slowing the rise of atmospheric CO₂ caused by fossil fuel burning. In 2023, this sink weakened, meaning land absorbed less CO₂ than in previous years, a concerning development for climate change mitigation.
The concept of a land carbon sink emerged in the 1980s when scientists realized that atmospheric CO₂ was rising slower than expected from fossil fuel emissions, implying an unidentified terrestrial uptake. This led to the 'missing sink' puzzle, later attributed to forest regrowth and CO₂ fertilization.
The sink operates on multiple timescales. In the short term, plants grow faster with more CO₂ (the CO₂ fertilization effect) and with longer growing seasons in a warming climate. Over decades, carbon accumulates in wood and soil organic matter. However, the sink is not guaranteed: droughts, fires, and heatwaves can kill vegetation or accelerate decomposition, turning land from a sink into a source. The 2023 weakening likely resulted from such stressors, possibly linked to an El Niño event that brought dry conditions to tropical regions, reducing photosynthesis and increasing respiration.
Quantifying the land sink is critical for carbon budgets and climate policy, as it determines how much emission reduction is needed to meet temperature targets.
The land carbon sink absorbs about 30% of human-caused CO₂ emissions, but its future is uncertain — if it weakens further, the pace of global warming could accelerate beyond current projections.










